Midterm 1 Flashcards
How have cities been show to alter the climate?
- increasing temperature
- decreasing relative humidity
- increasing cloudiness and fog
- decreasing solar radiation input
- decreasing overall wind speed
- increasing rainfall
- decreasing snowfall
What are the 5 major ways in which urban areas influence climate?
- Replacing grass, soil and trees with asphalt, concrete and glass
- Replacing rounded trees and bushes with angular buildings
- Introducing artificial heat (cars/buildings)
- Diverting water from infiltrating soul to drains and sewage pipes
- Releasing contaminants into the atmosphere
What is shortwave radiation?
Radiation with wavelengths between 0.15-3.0 micrometers
What is long-wave radiation?
Radiation with wavelengths between 3.0-100 micrometers
What is the Planetary Boundary Layer?
The portion of the atmosphere that is directly impacted by the underlying surface (Example: windspeed + direction, convection)
What is a Black Body?
Hypothetical object that’s surface emits the max amount of energy possible given its surface temperature. Found through Stefan-Boltzman Law
What are Grey Bodies?
The amount of energy emitted by a grey body can be found using the Stefan-Boltzman Law with the added parameter of emissivity
What does the Bowen Ratio express?
The proportion of energy that is used for sensible heat production relative to latent heat production
For Bowen Ratios greater than unity (1)…
…sensible heat is the main transfer and there is a limit to the available water
For Bowen Ratio less than unity (1)…
…latent heat is the main transfer and there is an increased water vapour content
What is the Urban Canopy Layer?
Vertical region extending from the surface to just above the roofs of buildings
What is the Urban Boundary Layer?
Vertical region extending from the Urban Canopy Layer to where the urban area no longer exerts an influence on the atmosphere
What are the conditions to create an Urban Canopy Heat Island?
Large city, clear skies, light winds, just after sunset
What are the components of the Urban Canopy Heat Island?
- Cliff
- Plateau
- Peak
What is the Cliff? (UCHI)
Found at the rural/urban boundary, it is an area with a steep temperature gradient.
What is the Plateau? (UCHI)
Area of study, but weaker horizontal temperature gradient towards the city centre. The uniformity of the plateau depends on urban land use
What is the Peak? (UCHI)
Located at the city core, is the area where the urban maximum temperature is found
How will the temperature change if the air is unsaturated?
The temperature change will be constant at the DALR of 0.98’C/100m
How will the temperature change if the air is saturated?
Will cool at a slower rate, the SALR= 0.65’C/100m (but it varies)
What is the Adiabatic rate?
Temperature changes with volume change
What is the Environmental Lapse Rate?
Approximately 6’C/km or 0.6’C/100m
What creates an unstable atmosphere?
When the ELR is greater than the DALR. This is common during sunny days when there is extreme surface heating
What creates a stable atmosphere?
When the ELR is less than DALR. An extremely stable atmosphere is when the ELR is negative
What creates a neutral atmosphere?
ELR is equal to DALR. Common during cloudy, windy conditions
What can limit the development of vertical temperature variations?
Clouds restrict surface heating and cooling
What are the 5 basic types of pollution plumes?
- Looping
- Coning
- Fanning
- Lofting
- Fumigation
What is Looping?
Strong instability. Occurs on fine summer days with large free convection (surface being heated). The loop is created by turbulent eddies that are larger than the plume diameter, thus the plume is carried up and down, and gets larger as it travels
How are looping plumes destroyed?
Destroyed at faster rate with increasing surface roughness and increasing wind speed
What is Coning?
Cloudy and windy conditions with stability close to neutral. Spreads in all directions equally due to turbulence and molecular diffusion
How are Coning plumes destroyed?
Since the cone gets larger downwind, the plume may hit the ground where there is no forced convection
What is Fanning?
Strongly stable atmosphere (eg. With an inversion). Turbulence is weak, thus little motion acting on the plume. Stable air keeps the plume from mixing and as a result the plume thins. May form v-shape when viewed from above
What is Lofting?
Occurs in the early evening when a nocturnal radiation inversion is building up from the surface. Moves pollutants upwards and is the “best” case scenario for ground level
What is Fumigation?
The opposite of lofting. Occurs when an inversion ‘lid’ obstructs upward dispersion of the plume, but unstable conditions allow for mixing below.